“…Apparently, the San Francisco volcanic field is quite complex, not unlike the Medicine Lake Highland field in northern California (Hughes 1982). Sanders et al (1982) arrived at similar conclusions in their more recent quantitative analysis of San Francisco field obsidians.…”
“…The obsidian sources within this field are, perhaps, the best studied in the Southwest (Jack 1971;Robinson 1913;Sanders et al 1982;Schreiber and Breed 1971). Although the chemical variability within sources in this field generally is less than in the mid-Tertiary sources to the south, the magmatic relations between some of these sources as previously reported probably are in error (Jack 1971;Sanders et al 1982). See Schreiber and Breed (1971: Figure 1) for a map of the field.…”
Section: San Francisco Volcanic Fieldmentioning
confidence: 99%
“…The nodules frequently were reduced at the source and flakes occur throughout the source area, but no intensive reduction areas were located. Published sources include Jack (1971), Moore et al (1960), Robinson (1913), Sanders et al (1982), Schreiber and Breed (1971). RS Hill.…”
Section: San Francisco Volcanic Fieldmentioning
confidence: 99%
“…With the advent of more efficient computer supported energy dispersive X-ray spectrometers, it now is possible to detect a number of elements simultaneously in the time it takes to analyze a few elements on the older manualwavelength instruments (Goffer 1980;Jenkins 1974;Macdonald 1980). With this spate of data, archaeologists turned to multivariate statistical techniques to determine assignments of archaeological information to source data (see Newman and Nielsen 1985;Sanders et al 1982). The problems here are complicated by both overlapping source data as above, and also by the problems of the many statistical and data assumptions inherent in multivariate techniques (Johnson and Wichern 1982).…”
Section: Quantitative and Semiquantitative Xrf Obsidian Studies In Armentioning
Comprehensive geochemical studies of archaeological obsidian sources in the Southwest typically have lagged behind other regions of North American and Mesoamerica. Current archaeological and petrological research indicates four previously unreported sources in Arizona, Sonora, and western New Mexico. This initial semiquantitative X-ray fluorescence (XRF) examination of archaeological silicic-glass sources in this region focuses on current technical problems in southwestern obsidian studies. The chemical variability within some regional obsidian sources appears to be relatively extensive and new data from the San Francisco volcanic field in northern Arizona modifies the results of earlier researchers.
“…Apparently, the San Francisco volcanic field is quite complex, not unlike the Medicine Lake Highland field in northern California (Hughes 1982). Sanders et al (1982) arrived at similar conclusions in their more recent quantitative analysis of San Francisco field obsidians.…”
“…The obsidian sources within this field are, perhaps, the best studied in the Southwest (Jack 1971;Robinson 1913;Sanders et al 1982;Schreiber and Breed 1971). Although the chemical variability within sources in this field generally is less than in the mid-Tertiary sources to the south, the magmatic relations between some of these sources as previously reported probably are in error (Jack 1971;Sanders et al 1982). See Schreiber and Breed (1971: Figure 1) for a map of the field.…”
Section: San Francisco Volcanic Fieldmentioning
confidence: 99%
“…The nodules frequently were reduced at the source and flakes occur throughout the source area, but no intensive reduction areas were located. Published sources include Jack (1971), Moore et al (1960), Robinson (1913), Sanders et al (1982), Schreiber and Breed (1971). RS Hill.…”
Section: San Francisco Volcanic Fieldmentioning
confidence: 99%
“…With the advent of more efficient computer supported energy dispersive X-ray spectrometers, it now is possible to detect a number of elements simultaneously in the time it takes to analyze a few elements on the older manualwavelength instruments (Goffer 1980;Jenkins 1974;Macdonald 1980). With this spate of data, archaeologists turned to multivariate statistical techniques to determine assignments of archaeological information to source data (see Newman and Nielsen 1985;Sanders et al 1982). The problems here are complicated by both overlapping source data as above, and also by the problems of the many statistical and data assumptions inherent in multivariate techniques (Johnson and Wichern 1982).…”
Section: Quantitative and Semiquantitative Xrf Obsidian Studies In Armentioning
Comprehensive geochemical studies of archaeological obsidian sources in the Southwest typically have lagged behind other regions of North American and Mesoamerica. Current archaeological and petrological research indicates four previously unreported sources in Arizona, Sonora, and western New Mexico. This initial semiquantitative X-ray fluorescence (XRF) examination of archaeological silicic-glass sources in this region focuses on current technical problems in southwestern obsidian studies. The chemical variability within some regional obsidian sources appears to be relatively extensive and new data from the San Francisco volcanic field in northern Arizona modifies the results of earlier researchers.
“…Archaeological obsidian research in the United States Southwest, until recently, has lagged significantly behind other regions (Shackley 1988(Shackley , 1995b. Not until the 1980s had significant petrological and geochemical research been available (Baugh and Nelson 1987; Hughes 1986, 1988Newman and Nielsen 1985Sanders et al 1982Shackley 1988, 1991, 1992, 1995bStevenson and Klimkiewicz 1990; see Shackley 1990 for a discussion of the history of research). Whereas a number of what seem to be minor sources of glass are appearing in archaeological contexts, most of the sources are known and characterized in the United States portion • of the Southwest (Shackley 1995b).…”
Section: Valle Del Azufre: Field Geologymentioning
Valle del Azufre is a newly discovered source of high-quality obsidian in central Baja California, which exhibits the most intensive exploitation of any known source in the greater United States Southwest and Northwest Mexico. Over 15 subsurface trenches and at least one adit occur at the source. Evidence for the prehistoric distribution of Valle del Azufre obsidian is presented based on energy-dispersive x-ray fluorescence spectrometry characterization of the source material and artifacts from the Baja California peninsula. Despite the intensity of exploitation at the source, the distribution of Valle del Azufre glass appears to be largely restricted to the central part of the peninsula.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.